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Stochastic inversion method of time-lapse controlled source electromagnetic data for CO2 plume monitoring

机译:CO2羽流监测时代延时控制源电磁数据的随机反转方法

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Carbon dioxide storage in deep saline aquifers can potentially reduce the CO2 concentration in the atmosphere due to anthropogenic activities with limited environmental impact. To minimize the risks of leakage, it is necessary to monitor the CO2 distribution in the reservoir. Here, we present a stochastic optimization method namely the Ensemble Smoother, to invert time-lapse marine controlled source electromagnetic data for predicting the CO2 plume location. Electromagnetic surveys have been successfully used in subsurface monitoring studies in different geosciences applications due to their sensitivity to the changes in the fluid in porous rocks. The inverse method is based on a Bayesian approach, in which an ensemble of stochastically generated prior models representing the spatial distribution of CO2 saturation is updated according to the mismatch between the measured data and the predicted electromagnetic response of the prior models. The proposed method generates an ensemble of updated realizations, the posterior models of the spatial distribution of CO2 saturation, that match the observations. The variance of the posterior models represents the uncertainty of the CO2 distribution. Compared to deterministic inversion methods, our proposed method is better suited to solve non-linear inverse problems with the added benefit of uncertainty quantification. The method is tested and validated on a real dataset, the Johansen formation, offshore Norway, for which we created synthetic time-lapse electromagnetic data for the entire injection period. The inversion of electromagnetic data shows that the proposed method can accurately predict the prediction of the CO2 plume location and quantify the associated uncertainty.
机译:由于具有有限的环境影响的人为活动,深盐含水层中的二氧化碳储存可能会降低大气中的CO2浓度。为了最大限度地减少泄漏的风险,有必要监测水库中的CO2分布。在这里,我们介绍了一个随机优化方法,即集合光滑,反转时间间隔船舶控制源电磁数据以预测CO2羽流量。由于它们对多孔岩石中的流体变化的敏感性,电磁调查已成功地用于不同地质应用中的地下监测研究。逆方法基于贝叶斯方法,其中根据所测量的数据与先前模型的预测电磁响应之间的不匹配来更新代表CO2饱和度的空间分布的随机产生的先前模型的集合。所提出的方法产生更新的实现的集合,二氧化碳饱和的空间分布的后模型与观测相匹配。后模型的方差代表了CO2分布的不确定性。与确定性反演方法相比,我们所提出的方法更适合解决非线性逆问题,以解决不确定性量化的增加的益处。该方法在实际数据集,约翰森组,离岸挪威进行了测试和验证,我们为整个注射期创建了合成时间流逝电磁数据。电磁数据的反转表明,该方法可以准确地预测CO2羽流位置的预测并量化相关的不确定性。

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